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TheoremStatement: Literature-sourcedProof: AI-adaptedPipeline-generatedprecheck passjudge pass (gpt-6-sol)audited 2026-09-30
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Variation field of a geodesic variation is a Jacobi field

Statement

Let (M,g) be a Riemannian manifold, let a<b, let ε>0, and let F:(−ε,ε)×[a,b]⟶M be a smooth geodesic variation, so every longitudinal curve t↦F(s,t) is an affinely parametrized geodesic. Set γ(t)=F(0,t),V(t)=∂sF(s,t)∣s=0. Then V is a Jacobi field along γ: Dt2V+R(V,γ˙)γ˙=0 on [a,b], using one-sided derivatives at included endpoints. No fixed endpoint condition is imposed; constant geodesics and dimension zero are included. This implication uses no axiom of choice.

Facts & Assumptions

Given: The supplied Riemannian manifold and smooth geodesic variation F:(−ε,ε)×[a,b]→M with a<b.

[F1]

A geodesic variation has central geodesic γ(t)=F(0,t) and variation field V(t)=∂sF(0,t); each longitudinal curve is affinely parametrized and satisfies Dt∂tF=0 (Geodesic variation).

[F2]

Along a smooth two-parameter map, covariant derivatives satisfy DsDtW−DtDsW=R(Fs,Ft)W for every smooth field W along the map (Covariant derivatives commute up to curvature in a two parameter variation).

[F3]

The Levi-Civita connection is torsion free: ∇XY−∇YX=[X,Y] (Levi civita connection).

[F4]

A smooth field J along γ is Jacobi when it satisfies Dt2J+R(J,γ˙)γ˙=0 (Jacobi field).

[F5]

Covariant differentiation along each parameter curve is defined by the induced pullback connection, for example DtW=(γ∗∇)∂/∂tW for a curve γ and a field W along it (Covariant derivative along a curve).

Proof

1.1F1F5given

Put S=Fs and T=Ft. By [F1], DtT=0 on the parameter rectangle, and the central variation field is V=S(0,⋅). Smoothness of F makes S and T smooth fields along F.

2.1F2step 1.1

Apply [F2] to the field T. Since DtT=0, 0=DsDtT=DtDsT+R(S,T)T, so DtDsT+R(S,T)T=0 throughout the rectangle.

3.1F2F3F4F5step 2.1

In local coordinates on M, torsion freeness [F3] and equality of the mixed partial derivatives of F give DsT=DtS: the ordinary mixed derivatives agree, and the connection terms cancel because the torsion is zero. Thus [F2] and [F3] imply Dt2S+R(S,T)T=0 for every s. At s=0, S=V and T=γ˙, so [F4] shows that V is Jacobi along γ.

4.1F1F4F5step 3.1∎

The equation holds on the interior and extends to included endpoints by smoothness up to t=a,b and the one-sided covariant derivatives. If V=0, the equation is immediate. If the central geodesic is constant, T(0,t)=0 and the same computation reduces to Dt2V=0. Empty M has no supplied variation; in dimension zero every field along F is zero; in dimension one the same calculation applies. The map F and its derivatives are supplied, and the proof uses no selection. This is a one-way implication, not an iff claim.

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